2002年3月21—22日影响韩国的沙尘天气分析

利用气象卫星、天气形势场和NCEP/NCAR再分析资料,分析了2002年3月21—22日影响韩国沙尘天气的原因。结果表明:影响韩国沙尘天气的沙尘主要源地是蒙古国和中国内蒙古地区。沙尘天气发生在地面冷锋后部,高压伸展的前面;19日和20日沙尘暴发生后,沙尘沿着西北风输送,21日早晨影响韩国;PM10最高值达到2 778.2μg/m³,由于西北风较强,沙尘暴发生后很快影响到韩国,但在韩国持续的时间较短。     

香港九龙大坑东地下蓄水方案数值研究

香港九龙大坑东地下蓄水方案(Tai Hang Tung Storage Scheme-THTSS)是香港西九龙渠道改善二期计划的一个重要组成部分,其目标是解决香港九龙繁华拥挤、人口稠密的商业中心旺角一带的洪水淹没问题。THTSS即是在经常洪水淹没区域(大坑东和界限街水渠交接处)上游足球场下面建立一个100 000 m3的地下蓄水池。本文建立了一个能处理明渠缓流和急流、封闭管道有压流、侧流堰和渠道汇合处过渡流于一体的一维水力数学模型,用1:22正态物理模型恒定流下的结果进行验证。数值模型计算了在50年一遇暴雨下,非恒定洪水在不同的侧流堰方案下的流动过程。结合物理模型试验结果,选择最佳的地下蓄水方案。计算结果表明,大坑东地下蓄水方案确实能加强旺角地区地洪水控制能力,并能通过50年一遇暴雨的洪水。     

一株海洋红法夫酵母Phaffia rhodozyma RP-306产虾青素的发酵条件优化

为提高海洋红法夫酵母Phaffia rhodozyma RP-306的虾青素产量,本研究利用单因素和响应面实验对其发酵条件进行了优化。首先用单因素实验确定了蔗糖、酵母粉、硫酸铵、pH、温度和装液量6个因素的初始值,再利用Plackett-Burman实验筛选出了影响较大的3个因素:蔗糖、pH、温度,并采用最陡爬坡实验确定了因素的合理范围,最后采用响应面法中的中心组合设计进行优化,其优化发酵条件为:蔗糖29.93 g/L,酵母粉2.0 g/L,硫酸铵5.0 g/L,pH 5.27,温度19.9℃。在此条件下虾青素产量从13.46 mg/L提高到17.04 mg/L,比优化前提高了26.61%。以优化后发酵条件进行分批发酵,虾青素产量达到28.86 mg/L,为进一步发酵放大研究奠定了良好基础。     

在EBEX-2000实验资料中湍流谱和局地各向同性特征

采用2000年8月在美国加州棉花地两个高度上应用超声三分量仪、快速响应050206 温度和湿度仪进行的EBEX-2000 (International Energy Balance Experiment,2000,EBEX-2000)风速三分量、温度和湿度湍流实验观测数据,计算分析了湍流速度、温度和湿度谱在不同稳定度下的特征.对湍流的局地各向同性进行了讨论并与Kansas和长白山原始森林湍流实验得到的结果进行了比较,得到了一些湍流特征量在不同下垫面情况下的一些有意义的特征.     

Local Meteorological and Synoptic Characteristics of Fogs Formed over Incheon International Airport in the West Coast of Korea

Fogs observed over Incheon international airport (IIA) in the westcoast of Korea from January 2002 to August 2006 are classified into categoriesof coastal fog, cold sea fog, and warm sea fog based on the areal extent of thefogs and the difference between the air temperature (T) and the SST, i.e.,cold sea fog if TSST = T-SST>0^oC and warm sea fog if TSST<0^oC. The numbers of coastal, cold, and warm sea fog casesare 64, 26, and 9. Coastal fogs form most frequently in winter, while cold seafogs occur mostly in summer and warm sea fogs are observed from January to Maybut not in November and December. On average the air gets colder by1.6^oC during the three hours leading up to the coastal fogformation, and an additional cooling of 1.1^oC occurs during thefog. The change in the dew point temperature (T_d) is minimal exceptduring the fog (0.6^oC). Decreases in T for the cold and warmsea fogs are relatively smaller. The average T_d is higher than SSTduring the cold sea fog periods but this T_d is more than4^oC higher than that for the corresponding non-fog days,suggesting that cold sea fogs be formed by the cooling of already humid air(i.e., T_d>SST). Increases of T_d are significant during thewarm sea fog periods (1.4^oC), implying that efficient moisturesupply is essential to warm sea fog formation. Four major synoptic patterns areidentified in association with the observed fogs. The most frequent is a northPacific high that accounts for 38% of cases. Surface or upper inversions arepresent in 77%, 69%, and 81% of the fog periods for coastal, cold, andwarm sea fogs, respectively.     

TEM and XRD determination of crystallite size and lattice strain as a function of illite crystallinity in pelitic rocks

Average crystallite size and mean-square strain of illite in rock specimens and clay separates were measured independently in TEM images and by single-line Fourier (Voigt method) profile analysis of the c. 1 nm peak of XRD patterns for a prograde sequence of pelitic rocks (illite crystallinity indices=0.17–0.58°Δ2θ) from the Gaspé Peninsula, Quebec. The TEM-determined crystallite sizes in clay separates approximate those determined by Fourier profile analyses and those calculated from illite crystallinity indices by the Scherrer equation, with the exception of the diagenetic sample. The crystallite sizes and mean-square strains of illite in rock samples exhibit a trend similar to that determined by profile analyses, but the average crystallite sizes are up to five times larger than those measured for clay separates. TEM images show that all rock samples have a wide range of crystallite sizes, and the proportions of larger crystallites increase with metamorphic grade. The diagenetic illite is defect-rich, fine-grained (mean thickness by volume=c. 70 nm), 1M_d material. Anchizonal illite tends to occur as separate aggregates of small 1M_d and larger 2M₁ crystals (c. 200 nm), comprising arrays of subparallel coalescing packets. The epizone sample has thick (c. 400 nm), defect-free crystals of muscovite occurring in stacks of parallel layers, or subhedral crystals intergrown with large-angle boundaries. Cleaved crystals that are free of intracrystalline layer terminations are dominant in clay separates of all samples, having ranges of smaller sizes with volume-average thicknesses of c. 43, 43, and 81 nm (c. 14, 28, 67 nm by the Voigt method), respectively, for the three zones. The results suggest that illite crystallinity indices do not provide a direct measure of a single microstructural state of illite in rocks, although they yield consistent limits for average crystallite sizes for the anchizone (23 & 48 nm here). Therefore, they serve as a general parameter of the degree of recrystallization on a relative basis, in part because the contributions of all peak-broadening variables (mixed layering, size and strain) decrease regularly with prograde regional metamorphism of pelites. The microstructural changes caused by rock disaggregation are probably a function of those variables as well. The data collectively demonstrate a trend from metastable, defect-rich, small crystals towards a stable assemblage of larger, defect-free crystals, through dissolution of strained crystals and neocrystallization, consistent with the Ostwald step rule.     

厚覆盖区找矿“循环渐近式勘查技术体系”与应用

覆盖区找矿难度不仅与覆盖层厚度有关,还与覆盖层物性、水文地质条件以及矿体特征关系密切。覆盖区找矿突破是一个系统过程,需要经历选区—圈靶—定位—验证评价4个阶段,存在勘查选区、地质信息探测和多学科有效融合难题。前人较少研究覆盖区找矿突破过程与勘查技术体系,笔者等基于"现有技术+结合实际创新"思路,总结提出了厚覆盖区找矿"循环渐近式勘查技术体系",在实际应用中,能够提高找矿成功率,入选自然资源部《矿产资源节约和综合利用先进适用技术目录(2019年版)》。